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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">OMEX2 North Atlantic Seasonal Sediment Trap Foraminifera Data</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Chapman, M.R.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Chapman, M.R.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleocean</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (OMEX2&gt;LATITUDE 49&gt;LONGITUDE -13)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Sediment trap samples from OMEX 2 (49°N, 13°W) provide a continuous 
record of the seasonal succession of planktonic foraminifera in the 
midlatitude North Atlantic and reveal a complex relationship between 
periods of production and specific hydrographic conditions. 
Neogloboquadrina pachyderma dextral coiling (d.), Globigerina bulloides, 
and Globorotalia inflata are found in great numbers during both the 
spring and summer seasons, whereas Globigerina quinqueloba, Globorotalia 
hirsuta, Globorotalia scitula, and Globigerinita glutinata are associated 
predominantly with the increase in productivity during the spring bloom. 
Globigerinella aequilateralis, Orbulina universa, and Globigerinoides 
sacculifer are restricted to late summer conditions following the 
establishment of a warm, well-stratified surface ocean. An annually 
integrated fauna from the sediment trap, comprising ~13,000 individuals, 
is used to evaluate the accuracy of five faunal-based statistical methods 
of paleotemperature estimation. All of the temperature reconstruction 
techniques produce estimates of ~16°C and ~11°C for summer and winter 
surface temperature, respectively, which are in excellent agreement 
with regional hydrographic data and suggest that the sediment trap 
assemblage is well represented in the core top faunas. Analysis of the 
key species that dominate the OMEX 2 sediment trap fauna, G. bulloides, 
G. inflata, and N. pachyderma d., based on d18O derived temperatures 
from North Atlantic core top samples, suggests that seasonal variations 
in planktonic foraminiferal production are nonuniform across the 
midlatitudes and that this is likely to complicate reconstructing 
past seasonal hydrographic dynamics using these taxa.


 
          STUDY NOTES: Sediment trap foraminifera data for the North Atlantic (49°N, 13°W) 
from the OMEX 2 project, at sub-seasonal resolution.   

</dc:description>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">NCDC-Paleoclimatology</dc:publisher>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce</dc:publisher>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Chapman, M.R.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2010-03-17</dc:date>
  <dc:type xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">ONLINE Files</dc:type>
  <dc:format xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">online, ASCII</dc:format>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/10456</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.txt</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.xls</dc:identifier>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.txt</dc:source>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.xls</dc:source>
  <dc:language xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">English</dc:language>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/10456</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.txt</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/chapman2010/chapman2010.xls</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Chapman, M.R. 2010.  
Seasonal production patterns of planktonic foraminifera 
in the NE Atlantic Ocean: Implications for paleotemperature 
and hydrographic reconstructions.  
Paleoceanography, 25, PA1101, doi:10.1029/2008PA001708. 

</dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 1993 AD  * END YEAR: 1994 AD</dc:coverage>
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   <ows:LowerCorner>-13  49</ows:LowerCorner>
   <ows:UpperCorner>-13  49</ows:UpperCorner>
  </ows:WGS84BoundingBox>
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